Detrital zircon geochronology and provenance of core sediments in Zhoulao Town, Jianghan plain, China

@article{Wang2010DetritalZG,
  title={Detrital zircon geochronology and provenance of core sediments in Zhoulao Town, Jianghan plain, China},
  author={Jietao Wang and Chang’an Li and Yong Yang and Lei Shao},
  journal={Journal of Earth Science},
  year={2010},
  volume={21},
  pages={257-271}
}
In our study, the U-Pb age spectrum of detrital zircons from terrigenous sediments is used to determine the sources. The Middle and Upper Reaches of the Yangtze River drain the western Yangtze craton and eastern Tibetan plateau, and take lots of sediments to the Jianghan (江汉) plain. Detrital zircons collected from Zhoulao (周老) core provide an ideal sample for the provenance studies. Here we report LA-ICP-MS U-Pb ages of 125 detrital zircons from one sand sample in the core sediments, which is… 

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References

SHOWING 1-10 OF 36 REFERENCES

Elemental compositions and monazite age patterns of core sediments in the

Precambrian crustal growth of Yangtze Craton as revealed by detrital zircon studies

Clastic sedimentary rocks are natural samples of the exposed continental crust over large areas. The age and evolution of the Yangtze craton is not well known, because much of the craton is covered

Identification of 3.5 Ga detrital zircons from Yangtze craton in South China and the implication for Archean crust evolution

Abstract The LA-ICP-MS U-Pb dating of hundreds of detrital zircon grains from the Sinian sandstones of Liantuo formation and tillites of Nantuo formation at Sanxia area in Yichang identified

Sampling Laurentia: Detrital zircon geochronology offers evidence for an extensive Neoproterozoic river system originating from the Grenville orogen

Neoproterozoic fluvial quartzarenites from the Shaler Group on Victoria Island in the western Canadian Arctic yield a diverse suite of detrital zircons. U-Pb ages from single zircons fall into three

Resistance of zircons to U–Pb resetting in a prograde metamorphic sequence of Caledonian age in East Greenland

In the Alpefjord area, Caledonian metamorphism from the chlorite zone to the sillimanite zone is seen to cut across the sedimentary pile of the lower Eleonore Bay Group. Zircons have been collected